Search results
Results from the WOW.Com Content Network
The lake has a storage capacity of 289,000 acre-feet (356,000,000 m 3), a normal surface area of 3,570 acres (1,440 ha) and a shoreline of 62 miles (100 km). The normal elevation is 733 feet (223 m) at the top of the conservation pool and 765 feet (233 m) at the top of the flood control pool. [4] The normal storage is 3116 acre-ft. [2]
In December 2019 the Central Highlands Regional Council made the decision to stay on level 1 water restrictions whilst they were undertaking a review of their trigger levels for water restrictions. [18] A record low of 7.39% was reached in 2020. [19] In late 2022, the dam reached 40% of capacity, allowing farmers to access full water ...
The river held at that level for two hours, but by then the level at the east end of the dam failed, sending the downstream river level 2 feet (0.61 m) higher in a matter of minutes. [8] By the time the crisis had passed, Jones, Oklahoma and Spencer, Oklahoma, two towns downstream of Oklahoma City, had been surrounded by water. The official ...
Lake Stanley Draper is a reservoir in southeast Oklahoma City, United States. It is one of three municipal reservoirs in the city. [a] Principal construction on the reservoir occurred between 1962-1963. Upon completion it was named after the long-time director of the Oklahoma City Chamber of Commerce, Stanley Draper. [3]
Canton Lake is a lake in Blaine and Dewey Counties in Oklahoma, near Longdale and Canton. Its main source of water is the North Canadian River. It is about an hour away from Enid. The lake serves as a municipal water supply reservoir for Oklahoma City, which pays to have water released from the lake for water-supply purposes. [2]
Get AOL Mail for FREE! Manage your email like never before with travel, photo & document views. Personalize your inbox with themes & tabs. You've Got Mail!
Oklahoma's Water by 2060 plan calls for Oklahoma to use "no more fresh water in 2060 than was used in 2012." [13] "Changing the climate is likely to increase the demand for water but make it less available. As rising temperatures increase evaporation and water use by plants, soils are likely to become even drier.
Central Oklahoma is a humid-subtropical region dominated by the Cross Timbers, an area of prairie and patches of forest at the eastern extent of the Great Plains. [2] The region is essentially a transition buffer between the wetter and more forested Eastern Oklahoma and the semi-arid high plains of Western Oklahoma, and experiences extreme swings between dry and wet weather patterns.